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We investigate how variations in a planet’s size and the chemical (mineral) composition of its upper mantle and surface affect processes involved in the carbonate-silicate cycle, which is thought to have regulated the composition of Earth’s atmos
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ef3fe2e9a3ed323b06053343cb31c8d6
https://doi.org/10.22541/essoar.167751627.79222663/v1
https://doi.org/10.22541/essoar.167751627.79222663/v1